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Divergences such as braided streams actually maintain the same order all the way through the braid, just like it was a single stream; however, divergences that are not braided streams keep the upstream order number and follow the normal hierarchy further downstream. Horton, R. E. (1945), \"Erosional development of streams and their drainage basins: hydro-physical approach to quantitative morphology\", Geological Society of America Bulletin 56 (3): 275\u2013370. Strahler, A. N. (1952), \"Hypsometric (area-altitude) analysis of erosional topology\", Geological Society of America Bulletin 63 (11): 1117\u20131142. https://usgs-mrs.cr.usgs.gov/NHDHelp/WebHelp/NHD_Help/Introduction_to_the_NHD/Feature_Attribution/Stream_Order.htm", "mapName": "Layers", "description": "", "copyrightText": "USGS", "supportsDynamicLayers": true, "layers": [ { "id": 0, "name": "Rivers (all)", "parentLayerId": -1, "defaultVisibility": false, "subLayerIds": null, "minScale": 0, "maxScale": 0 }, { "id": 1, "name": "Rivers (major)", "parentLayerId": -1, "defaultVisibility": true, "subLayerIds": null, "minScale": 0, "maxScale": 0 }, { "id": 2, "name": "Rivers (subbasin level)", "parentLayerId": -1, "defaultVisibility": true, "subLayerIds": null, "minScale": 0, "maxScale": 0 }, { "id": 3, "name": "Rivers (watershed level)", "parentLayerId": -1, "defaultVisibility": false, "subLayerIds": null, "minScale": 0, "maxScale": 0 }, { "id": 4, "name": "Rivers (subwatershed level)", "parentLayerId": -1, "defaultVisibility": false, "subLayerIds": null, "minScale": 0, "maxScale": 0 }, { "id": 5, "name": "Waterbodies", "parentLayerId": -1, "defaultVisibility": false, "subLayerIds": null, "minScale": 0, "maxScale": 0 } ], "tables": [], "spatialReference": { "wkid": 4269, "latestWkid": 4269 }, "singleFusedMapCache": false, "initialExtent": { "xmin": -125.28240701006844, "ymin": 38.6936118123577, "xmax": -109.37428631142267, "ymax": 49.81038307997146, "spatialReference": { "wkid": 4269, "latestWkid": 4269 } }, "fullExtent": { "xmin": -124.72442391684274, "ymin": 32.51016838640893, "xmax": -109.7705582067208, "ymax": 49.039371405131135, "spatialReference": { "wkid": 4269, "latestWkid": 4269 } }, "minScale": 0, "maxScale": 0, "units": "esriDecimalDegrees", "supportedImageFormatTypes": "PNG32,PNG24,PNG,JPG,DIB,TIFF,EMF,PS,PDF,GIF,SVG,SVGZ,BMP", "documentInfo": { "Title": "NHD2012", "Author": "Shanna Dunn, GIS Analyst, Protected Resources Division", "Comments": "The West Coast Region leverages the National Hydrography Dataset as a base dataset for managing marine and anadromous species. 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Divergences such as braided streams actually maintain the same order all the way through the braid, just like it was a single stream; however, divergences that are not braided streams keep the upstream order number and follow the normal hierarchy further downstream. Horton, R. E. (1945), \"Erosional development of streams and their drainage basins: hydro-physical approach to quantitative morphology\", Geological Society of America Bulletin 56 (3): 275\u2013370. Strahler, A. N. 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